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doi:10.5194/se-2016-123
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
31 Aug 2016
Review status
A revision of this discussion paper for further review has not been submitted.
First magmatism in the New England Orogen, Australia: Forearc and arc-backarc components in the Bakers Creek Suite gabbros
Seann J. McKibbin1,2,a, Bill Landenberger1, and Mark C. Fanning2 1School of Environmental and Life Sciences, University of Newcastle, Uni versity Drive, Callaghan, 2308, Australia
2Research School of Earth Sciences, Australian National University, Bldg. 61, Mills Road, Canberra, 0200, Australia
anow at: Analytical, Environmental and Geo-Chemistry, Vrije Universiteit Brussel, Pleinlaan 2, Bru ssels 1050, Belgium
Abstract. The New England Orogen, Eastern Australia, was established as an outboard extension of the Lachlan Orogen through the migration of magmatism into the forearc basin and accretionary prism. Widespread S-type granitic rocks of the Hillgrove and Bundarra Supersuites represent the first pulse of magmatism, followed by I- and A-types typical of circum-Pacific extensional accretionary orogens. Associated with the former are a number of small tholeiite-gabbroic to intermediate bodies of the Bakers Creek Suite, which are a heat source for production of granitic magmas and potential tectonic markers indicating why magmatism moved into the forearc and accretionary complexes, rather than rifting the old Lachlan Orogen arc. The Bakers Creek suite gabbros capture an early (~ 305 Ma) forearc basalt-like component with low Th/Nb and with high Y/Zr and Ba/La, recording melting in the mantle wedge with little involvement of a slab flux and indicating forearc rifting. Subsequently, arc-backarc like gabbroic magmas (305–304 Ma) were emplaced followed by diverse magmatism of mixed compositions leading up to the main S-type granitic intrusion (~ 290 Ma). This trend in magmatic evolution implicates forearc and other mantle wedge melts in the heating and melting of fertile accretion complex sediments and relatively long (~ 10 Myr) timescales for such melting.

Citation: McKibbin, S. J., Landenberger, B., and Fanning, M. C.: First magmatism in the New England Orogen, Australia: Forearc and arc-backarc components in the Bakers Creek Suite gabbros, Solid Earth Discuss., doi:10.5194/se-2016-123, in review, 2016.
Seann J. McKibbin et al.
Seann J. McKibbin et al.

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Short summary
The youngest, eastern-most part of continental Australia formed in an ancient subduction zone by rifting of the crust. This drove melting of the underlying mantle, producing basaltic magmas that intruded the crust. We determined the composition and ages of these intrusives, finding that they predate other types of magma in the area. This indicates a progression in magma types from basaltic (mantle origin), through mixed, to granitic (crust recycling) during the growth of this region.
The youngest, eastern-most part of continental Australia formed in an ancient subduction zone by...
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